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Mongolian Plateau facts for kids

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Mongolian Plateau
Mongolian Plateau
Mongolei-Topografie,Atlas1903.JPG
1903 topographic map of the Qing dynasty depicting the Mongolian Plateau
Chinese name
Chinese 蒙古高原
Mongolian name
Mongolian Cyrillic Монголын тэгш өндөрлөг
Mongolian script ᠮᠣᠩᠭᠣᠯ ᠤᠨ
ᠲᠡᠭᠰᠢ
ᠥᠨᠳᠥᠷᠯᠢᠭ

The Mongolian Plateau is the part of the Central Asian Plateau lying between 37°46′-53°08′N and 87°40′-122°15′E and having an area of approximately 3,200,000 square kilometres (1,200,000 sq mi). It is bounded by the Greater Hinggan Mountains in the east, the Yin Mountains to the south, the Altai Mountains to the west, and the Sayan and Khentii mountains to the north. The plateau includes the Gobi Desert as well as dry steppe regions. It has an elevation of roughly 1,000 to 1,500 meters, with the lowest point in Hulunbuir and the highest point in the Altai.

Politically, the plateau spans all of Mongolia, along with parts of China and Russia. Inner Mongolia and parts of the Dzungarian basin in Xinjiang encompass the Chinese portion of the plateau. In Russia, the plateau forms Transbaikal, part of Buryatia, and the southern Irkutsk Oblast.

History

The plateau was inhabited and conquered by various groups, including (chronologically) the Xiongnu, Xianbei, Göktürks, Tang dynasty, Liao dynasty, Mongol Empire, Yuan dynasty, Northern Yuan dynasty, and Qing dynasty.

Changing environment

Between 1980 and 2010, rising global temperatures and direct human activity (particularly the use of lake water for mining and agriculture) have contributed to a significant loss of lake surface area across the Plateau. Qagaan Nurr and XinKai Lake have shrunk by two-thirds of their surface area during that time, while others (including Huangqihai Lake and Naiman Xihu) have dried up entirely. Some exceptions, such as East Juyan Lake and Had Paozi, have grown, but overall the average total surface area of lakes in the region has shrunk by 30%.

See also

Kids robot.svg In Spanish: Meseta de Mongolia para niños

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